Ž–¼ | ˜_•¶‘è–Ú | —vŽ| |
Tae-Ho PARK | Chronological and Petrological Study of Cretaceous to Paleogene Granitic Rocks, South Korea | |
‰ª“c ^‰î | Crustal extension and shortening in the back-arc region of Northeast
Japan | |
òŽR “O–ç | Incremental melting process and thermal evolution of an upwelling mantle: constraints from back arc volcanisms in the eastern margin of the Eurasian Plate
| |
“ào ’•F | Observational study on the self-similarity of earthquake rupture growth in Parkfield area | |
²“¡ —FŽq | SiO2 ƒKƒ‰ƒX‚Ì–§“x‚Æ\‘¢‚Ì’´‚ˆ³‰º‚»‚Ìꑪ’è | |
–ì“c Žé”ü | GPS Data Inversion to Estimate 3-D Elastic/Inelastic Strain Fields in Island-Arc Crust | |
ŽRŒû ”ò’¹ | Linkage between faulting, fluid flow and earthquake generation in seismogenic subduction zones | |
Ž–¼ | ˜_•¶‘è–Ú | Žw“±‹³Š¯ |
ŒIŒ´ ‹`Ž¡ | Statistical analysis of seismicity by discretized triggering model i—£ŽU“IƒgƒŠƒKƒŠƒ“ƒOƒ‚ƒfƒ‹‚É‚æ‚é’nkŠˆ“®‚Ì“Œv“I‰ðÍj | ˆäo “N |
‰––¡ —I–ç | Æ«/‘Y«‘JˆÚ—̈æ‚É‚¨‚¯‚é™’’f‘Ñ‚Ì”ñ‘ÎÌ«‚ɂ‚¢‚Ä‚ÌlŽ@ | “c’† GŽÀ |
¼ŽR Œ’Žu | Analysis of Size, Geometry, and Motion of PlatesiƒvƒŒ[ƒg‚̃TƒCƒYAŒ`A‰^“®‚̉ðÍj | –Ø‘º Šw |
–ƒ¶ ®•¶ | Intraplate Deep Low Frequency Earthquakes far from Active Volcanoes iŠˆ‰ÎŽR‚©‚ç—£‚ꂽƒvƒŒ[ƒg“à‚Ì[•”’áŽü”g’nkj | ˆäo “N |
‚“c Œ[l | ’á–§“xSiO2 Œ‹»‚̃wƒŠƒEƒ€’†‚ł̈³k‹““® | ‘DŽç “W³ |
’·’Jì Œc | Seismic Waveform Evidence for Existence of an Ultra-low Velocity Zone with Significant Amounts of Iron in the lowermost mantle beneath the central Pacific (’nk”gŒ`•ªÍ‚©‚玦´‚³‚ê‚é’†‰›‘¾•½—m‰ºƒ}ƒ“ƒgƒ‹Å‰º•”‚É‚¨‚¯‚é’´’ᑬ“x—̈æ‚Ì‘¶Ý) | ƒQƒ‰[ ƒƒo[ƒg |
”ä–¼ ËŽq | Dehydration and deformation processes of siliceous sediments in subduction zonesi’¾‚Ýž‚Ý‘Ñ‚É‚¨‚¯‚éŒ]Ž¿‘ÍÏ•¨‚Ì’E…E•ÏŒ`‰ß’öj | –Ø‘º Šw |
Žá—Ñ ‘å—C | ‚–§“x‰»SiO2 ƒKƒ‰ƒX‚̈³k‹““® | ‘DŽç “W³ |
Ž–¼ | ˜_•¶‘è–Ú | Žw“±‹³Š¯ |
‘¾“c ˜aW | Precise hypocenter distribution of deep low-frequency earthquakes and its relationship to the local geometry of the subducting plate in Nankai subduction zone, Japan (“ìŠCƒgƒ‰ƒt’¾‚Ýž‚Ý‘Ñ‚É‚¨‚¯‚é[•”’áŽü”g’nk‚̸–§kŒ¹•ª•z‚Æ‹ÇŠ“I‚ȃvƒŒ[ƒg\‘¢‚Æ‚ÌŠÖŒW) | ˆäo “N |
“í“c ç•ä | Geochemical and numerical studies on slab-derived fluids and the Arima-type brine (ƒXƒ‰ƒu‹NŒ¹—¬‘Ì‚Æ—L”nŒ^‰–…‚ÉŠÖ‚·‚é’n‹…‰»Šw ‚¨‚æ‚Ñ”’lƒ‚ƒfƒŠƒ“ƒOŒ¤‹†) | ŠâX Œõ |
¬¼ Œ’‰î | Shear velocity structure in the lowermost mantle beneath the western Pacific from waveform inversion i”gŒ`ƒCƒ“ƒo[ƒWƒ‡ƒ“‚É‚æ‚鼑¾•½—m‰º‚Ìʼnº•”ƒ}ƒ“ƒg ƒ‹S ”g‘¬“x\‘¢„’èj | ƒQƒ‰[ ƒƒo[ƒg |
¬—Ñ ¡“úŽq | Diagenesis, dehydration and deformation of pelagic sediments in ancient subduction zone inferred from bedded chert in the Inuyama area, Mino Belt i’¾‚Ý ž‚Ý‘Ñ‚É‚¨‚¯‚éƒ`ƒƒ[ƒg‘w‚Ì‘±¬E’E…‚Æ•ÏŒ`‚ÌŠÖŒW-”ü”Z‘ÑŒ¢ŽR’nˆæ‚æ‚è-j | –Ø‘º Šw |
–ì’à ‘¾ˆê | Particle Analysis and Energetics of Fault Rocks: An Example from the Toyamagawa Fault, Central Japan i’·–쌧‰“ŽRì’f‘w‚ð—á‚Æ‚µ‚½C’f‘wŠâ‚Ì—±Žq‰ðÍ‹y‚уGƒlƒ‹ƒM[˜_j | “c’† GŽÀ |
Ž–¼ | ˜_•¶‘è–Ú | Žw“±‹³Š¯ |
‰iˆä GŒ› | Experimental Study of Pressure Effects on Microstructure of Partially-Molten Forsterite-Jadeite System i•”•ª—n—ZƒtƒHƒ‹ƒXƒeƒ‰ƒCƒg[ƒqƒXƒC‹PÎŒn‚Ì”÷×\‘¢‚ւ̈³—ÍŒø‰Ê‚ÌŽÀŒ±“IŒ¤‹†j | ¬àV ˆêm |
㞊 —T‹v | ’PŽÎ‹P΃|[ƒtƒBƒƒNƒ‰ƒXƒg‚ð—p‚¢‚½ƒ}ƒ“ƒgƒ‹‚©‚ñ‚ç‚ñŠâ‚̉·“x-ˆ³—Í-•ÏŒ`Žw•W `–y–ž‚©‚ñ‚ç‚ñŠâ‘Ì‚Ì㸗š—ð‚Ö‚Ì“K‰ž | ¬àV ˆêm |
‘—t —zŽq | Shear zone growth on the splay fault in accretionary prism |the footwall of the Nobeoka Thrust in the Shimanto Belt (‹ãBŽl–œ\‘щ„‰ªÕã’f‘w‚©‚猩‚éout-of-sequence- thrust‚Ì™’’f‘Ñ‚Ì”’B) | –Ø‘º Šw |
œAì ’q—² | Õ’Ãì’f‘w‚É‚¨‚¯‚é, ”÷¬’nk‘½”/‹ó”’—̈æ‚Ì’f‘wŠâ”äŠrŒ¤‹† | “c’† GŽÀ |
–kžŠ ˆ¤ | Deformation and diagenesis of sandstones in underthrusted sediments -An example from the Mugi Melange, Shikoku, Japan- i•t‰Á‘Ì’†‚Ì‘ÍÏ•¨‚ªŽó‚¯‚鑱¬‚¨‚æ‚Ñ•ÏŒ`‰ß’ö-Žl–œ\‘Ñ–´Šòƒƒ‰ƒ“ƒWƒ…‚Ì—á-j | –Ø‘º Šw |
¼”ö r•F | ƒ_ƒCƒ„ƒ‚ƒ“ƒhƒAƒ“ƒrƒ‹‘•’u—pc-BNƒKƒXƒPƒbƒgŠJ”‚Æ‚»‚̉ž—p | ‘DŽç “W³ |
Ž–¼ | ˜_•¶‘è–Ú | Žw“±‹³Š¯ |
ã–Ø Œ«‘¾ | Subduction zone magmatism and mantle wedge structure of the Sengan region, Northeastern Japan | ŠâX Œõ |
“ào ’•F | Development of Multiscale Slip Inversion Method and Its Application to the 2004 Mid-Niigata Prefecture Earthquake | ˆäo “N |
‰Y“c ‹IŽq | ƒ_ƒCƒŒ[ƒ^ƒ“ƒV[‚ðl—¶‚µ‚½thermal pressurization ƒ‚ƒfƒ‹‚Ì’nk’f‘w‚Ö‚Ì“K—p-–쓇’f‘wAŽÔâÄš¼’f‘w‚ð—á‚É‚µ‚Ä- | “c’† GŽÀ |
¬“c W | ˆÉ“ß’J’f‘w‘Ñ‚Ì\‘¢‚Æ‚»‚Ì”’B‰ß’ö | ’r“c ˆÀ—² |
¬“c“‡ —f_ | Cr-Al spinel as a deformation indicator for the upper mantle: observational study in the Horoman Peridotite Complex | ¬àV ˆêm |
²“¡ —FŽq | ’´‚ˆ³‰º‚É‚¨‚¯‚é“ñŽ_‰»•¨‚Ìpost-PbCl2 ‘Š“]ˆÚ‚ÌŒ¤‹† | ‘DŽç “W³ |
–ì“c Žé”ü | Inversion Analysis of Geodetic Data in the Kanto Region, Central Japan, with a 3-D Plate Interface Model: Diversity of Stress Release Modes | ¼‰Y [G |
ŽRŒû ”ò’¹ | The origin of syntectonic veins in accretionary complex and its implication for fluid behavior around the up-dip limit of seismogenic zone | –Ø‘º Šw |
Ž–¼ | ˜_•¶‘è–Ú | Žw“±‹³Š¯ |
‰¬’à ’B | Mechanisms of crustal differentiation of basaltic magmas: Constraints from the contrasting variation trends observed in Aogashima and@other Izu Arc volcanoes Œº•ŠâŽ¿ƒ}ƒOƒ}‚Ì’nŠk“à•ª‰»ƒƒJƒjƒYƒ€Fƒ–“‡‚¨‚æ‚шɓ¤ŒÊ‰ÎŽR‚É‚Ý‚ç‚ê‚é‘ÎÆ“I‚ȕω»ƒgƒŒƒ“ƒh‚©‚ç‚̧–ñ | ¬àV ˆêm |
‰Í‡ Œ¤Žu | The Direct Solution Method for computing synthetic seismograms in transversely isotropic spherically symmetric media and its applications | ƒQƒ‰[ ƒƒo[ƒg |
ì’[ ŒP‘ã | Apllication of the isocon method to argillaceous rocks of accretionary complex and@quantitavive estimation of volume change due to mass transfer associated with deformation i•t‰Á‘Ì“DŽ¿Šâ‚Ö‚Ìisocon–@‚Ì“K—p‚Æ•ÏŒ`‚É”º‚¤Ž¿—ʈړ®‚É‚æ‚é‘Ìϕω»‚Ì’è—Ê“IŒ©Ï‚à‚èj | –Ø‘º Šw |
–k‘º —Lv | Magnetic fabric of underplated melange and its relationship with lithology of the@Shimanto Belt, southwest Japan i¼“ì“ú–{AŽl–œ\‘Ñ‚ÉŒ©‚é’ꂯƒƒ‰ƒ“ƒWƒ…‚ÌŽ¥«ƒtƒ@ƒuƒŠƒbƒN‚ÆŠâ‘Š‚Æ‚ÌŠÖŒWj | –Ø‘º Šw |
Ž›ì ŽõŽq | ƒTƒ“ƒAƒ“ƒhƒŒƒAƒXŒ^‰¡‚¸‚êƒvƒŒ[ƒg‹«ŠE‚Ìâ‘΋“x„’è | ¼‰Y [G |
’†‘º m”ü | —¼”’ŽR’n‚É‚¨‚¯‚é’¾‚Ýž‚ݑщάŠˆ“® | ŠâX Œõ |
•Ÿˆä Œ’Žj | Development of a 3D Standard Model of Plate Interfaces in and around Japan: Physical Interpretation of Long-term Crustal@Movements in Kanto District i“ú–{—ñ“‡ˆæ‚ÌŽOŽŸŒ³ƒvƒŒ[ƒg‹«ŠEŒ`󃂃fƒ‹‚Ì\’zFŠÖ“Œ’nˆæ‚Ì’·Šú“I’nŠk•ÏŒ`‰^ “®‚̉ð–¾j | ¼‰Y [G |
¼‘º ³”V | P-T condition and heterogeneous fluid flow through cracks in the underthrusted melange- observation from the Shimanto Belt, Japan i’¾‚Ýž‚ñ‚¾ƒƒ‰ƒ“ƒWƒ…‚É‚¨‚¯‚銄‚ê–Ú‚ð’Ê‚µ‚½•s‹ÏŽ¿‚È—¬‘Ì‚Ì—¬‚ê‚Ɖ·“xEˆ³—ÍðŒ[Žl–œ\‘Ñ ‚Å‚ÌŠÏŽ@j | –Ø‘º Šw |
ŽR–{ Žu”T | Xü‰ñÜ–@‚É‚æ‚éMgSiO3ƒƒ‹ƒg‚ÆCaSiO3ƒƒ‹ƒg‚Ì\‘¢‚̈³—͕ω»‚ÌŒ¤‹† | ‘DŽç “W³ |
DJURAEV Omon | Efficient and accurate methods for evaluating analytic solutions of the elastic equation of motion and their application to data analysis i‚¸“x‹y‚Ñ‚ŒvŽZ”\—¦‚ð—L‚·‚é’e«‘̂̉^“®•û’öŽ®‚̉ðÍ“I‰ð‚«•û‚Æ‚»‚̉ž—pj | ƒQƒ‰[ ƒƒo[ƒg |